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The Golden Circle is a 300 kilometre (186 mile) route to the three most popular natural attractions in Iceland: the Geysir Geothermal Area, Gullfoss Waterfall and Þingvellir National Park.

This sightseeing trail is easy to do within half a day from Reykjavík, either by self-drive or on one of many tours. Some of these tours have additional activities, such as snorkelling or snowmobiling, or are conducted in a unique style, such as by helicopter, or under the midnight sun.

Within the three locations of the Golden Circle are some of the clearest examples of Iceland’s fascinating geological forces, magnificent landscapes, and rich culture.

The Geysir Geothermal Area

Though this feature is currently in a phase of inactivity, its neighbour Strokkur more than makes up for it. Every five to ten minutes, it blasts a column of boiling water to heights that can reach over 40 metres (131 feet).

The surrounding area is dotted with fumaroles, hot springs, and mud-pits. There are also two other smaller geysers, Smiður and Litlí-Strokkur, that can be easily visited, as well as a hotel, restaurant, cafe and gift shop across the road.

Gullfoss Waterfall

The 'Golden Waterfall', Gullfoss one of the most beautiful and powerful waterfalls in Iceland, plummeting 32 metres (105 feet) in two tiers into the river gorge of the popular rafting river Hvítá. It is just a ten-minute drive from Geysir and is the furthest point on the Golden Circle from Reykjavík.

Gullfoss was very almost lost in the early 20th century when British developers sought to harness its incredible power for geothermal energy. Though they got the lease to the land, allowing them to go ahead with their plans, they met an unlikely adversary: the daughter of the farmer who owned it, Sigríður Tómasdóttir.

This resilient woman refused to see the waterfall, to which she and her sisters paved the first path, destroyed. She, therefore, walked over 200 kilometres (124 miles) to Reykjavík and back multiple times to meet with a lawyer in order to help change the decision.

Though the process was arduous and took years, eventually Sigríður managed to exhaust the resources of the businessmen and they withdrew their plans. Because of her, all Icelandic waterfalls are now protected from foreign investors, and she is considered one of Iceland’s first environmentalists and most important historical people.

Thingvellir National Park

The largest attraction of the Golden Circle is Þingvellir National Park. The Icelandic parliament was founded here in 930 and remained until the year 1798 before moving to Reykjavík, making it the original site of what is now the world’s longest ongoing parliament.

Today it is a UNESCO World Heritage Site and one of the most important places to visit in Iceland. This is not just for its historical and cultural values, but for also its magnificent landscape and dramatic geology.

Þingvellir is surrounded by a beautiful mountain and volcanic ranges, as it is located in a rift valley directly between the North American and Eurasian tectonic plates. This makes it one of the few places in the world where you can walk between the continents, in the Mid-Atlantic Rift.

The daring and qualified even have opportunities to snorkel or scuba dive in this no-mans-land, in a ravine filled with crystal-clear spring water called Silfra. The visibility here can exceed 100 metres (328 feet), revealing incredible geological sites. Though it never freezes over due to the constant flow of water into it, it is 2°C (35°C) throughout the year, thus underwater explorers are always equipped with protective suits.

Other sites of note are the magnificent Almannagjá gorge, which you can walk down into to reach the rift valley from the North American tectonic plate, and the beautiful lake Þingvallavatn, the largest lake in Iceland, which gleams to the south of the National Park.

Reykjavík is the capital of Iceland and the northernmost capital of any sovereign state in the world.

Despite a small population (approximately 120,000, with just over 200,000 in the Greater Reykjavík area), it is a vibrant city that draws an ever increasing number of visitors every year. It is the financial, cultural and political centre of Iceland, and has a reputation of being one of the cleanest and safest cities in the world.

Geography

The city of Reykjavík is located in southwest Iceland by Faxaflói Bay. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal; after all, its name translates to ‘Smoky Bay’.

Much of the current city area was subglacial during the Ice Age, with the glacier reaching as far as the Álftanes peninsula, while other areas lay under the sea. After the end of the Ice Age, the land rose as the glaciers drifted away, and it began to take on its present form.

The coastline of Reykjavík is set with peninsulas, coves, straits and islands, most notably the island of Viðey, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful.

Mount Esjan is the highest mountain in the vicinity of Reykjavík and the most distinctive feature of the coastline. This majestic summit is also highly popular amongst hikers and climbers. Other notable mountains that can be seen from the seaside are Akrafjall and Skarðsheiði.

The largest river to run through the city is Elliðaá in Elliðaárdalur valley, which is also one of Iceland’s best rivers for salmon fishing.

Transportation

There are no trains or trams in Iceland, but most people travel by car. The city also operates a bus system. There are two major harbours in town, the old harbour in the centre and Sundahöfn in the east.

The domestic Reykjavík Airport is located at Vatnsmýrin, not far from the city centre and close to the hill Öskjuhlíð and the restaurant, vantage point and exhibition centre Perlan. The international Keflavík Airport at Miðnesheiði heath then lies around 50 kilometres (31 miles) from the city.

Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered. It is, however, quite easy to walk between the major sites.

What to See & Do in Reykjavik

The local arts scene is strong in Iceland, with annual events and festivals, many of artists from which have hit the international stage.

Major events taking place in Reykjavík include Iceland Airwaves, Reykjavík Pride, RIFF (The Reykjavík International Film Festival), The Reykjavík Literature Festival, Culture Night, the Reykjavík Arts Festival, Food & Fun, the Reykjavík Fashion Festival and the Sónar music festival.

Those eager to soak up the local culture should visit the city’s many museums, exhibitions and galleries, and check out live music at the cafés, bars, and concert venues dotted around. You could look at the programmes of what’s on at the Harpa music hall or the theatres, or else plan a few hours at the lighthouse at Grótta, the shopping street of Laugavegur, or the old harbour and the flea market.

You could even book a bird- and whale watching tour or a visit to Viðey island. There are a lot of things to do and the possibilities are endless.

Make sure to visit the public square of Austurvöllur, one of the city’s most popular gathering places, where you’ll also find the national parliament, the Alþingi, as well as the state church, a statue of independence hero Jón Sigurðsson, cafés, bars and restaurants.

Austurvöllur was central in the protests following the banking collapse of 2008, along with Lækjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrímskirkja that towers over the city from the hill of Skólavörðuholt, from which you’ll get a great view of the city.

Try a walk by the city pond, Tjörnin, to greet the many birds that frequent the area and to visit the city hall, stationed by its banks. A beautiful park lies by the pond, ideal for a nice walk, and sometimes concerts get held there.

Further off is the campus of the University of Iceland, the Nordic house and the Vatnsmýrin wetland, a particularly pleasant place, but be mindful to not disturb the wildlife there by keeping to the pathways.

For a nice swim on a warm day, we particularly recommend Nauthólsvík beach, which is heated with geothermal water. Those who love a dip should also visit the Laugardalur valley, home to one of the city’s best swimming pools, which sits a short walk away from Ásmundarsafn gallery, a beautiful botanical garden and a domestic zoo.

A walk by the Ægissíða beach, with its old fishing sheds, in the west part of Reykjavík also holds a particular charm. From there, you can see all the way to president’s house at Bessastaðir, which is also a historical site in its own right, having been the educational centre of Iceland for centuries.

Another place that offers one of the city’s best views is Perlan, up on Öskjuhlíð hill. The hill itself is a popular place to spend a few hours, with over 176,000 trees and great opportunities for walking and cycling. Perlan also has and observation deck with great views, a café and an exhibition centre.

Finally, we’d like to stress that these are only some suggestions of the many things you might check out in Reykjavík. Whatever you choose to do, we hope you’ll be able to make the most of your visit and we wish you a pleasant stay in our capital.

Faxaflói is a large bay in west Iceland, between the Reykjanes and Snӕfellsnes Peninsula. It faces Reykjavík, and is a hot spot for puffin and whale watching.

Activities in Faxaflói Bay

Whale watching tours head into Faxaflói from Reykjavík throughout the year. Throughout the summer, the most commonly seen species are Minke and Humpback whales, while Harbour Porpoises and White-Beaked Dolphins are seen year-round. Other species are seen on occasion, including Orcas and Blue Whales.

From May to September, some of these tours include a puffin-watching segment to the islands of Lundey and Akurey, where visitors can see them nesting on the rocks and bobbing in the water.

Another island, Viðey, can easily be visited throughout the year by boat, with tickets included on the Reykjavík City Card. It is home to the Yoko Ono Peace Tower.

Sea-angling is also popular in Faxaflói, and it is possible to rent a rod and fish from Reykjavík Harbour.

Faxaflói Bay from Reykjavík

Faxaflói Bay is a beautiful feature of Iceland’s capital, visible from much of the city. Many of Reykjavík’s greatest landmarks have it as their backdrop, as they hug the coastline.

Harpa Concert Hall, for example, is an incredible feat of modern architecture that juts out into the water. The Sun Voyager is a popular statue that also looks out to the sea.

In decent weather, visitors can see some of Iceland’s most beautiful nature across Faxaflói. Mount Esjan is the most dominant feature, but when it is especially clear, it is possible to see the Reykjanes and Snӕfellsnes Peninsulas.

Skogafoss is one of the biggest and most beautiful waterfalls of the island with an astounding width of 25 meters and a drop of 60 meters.

This is one of the most popular waterfalls in Iceland for travellers to visit. It is located in South Iceland, not far from Skogar, which itself features a highly interesting regional museum. Due to the amount of spray the waterfall often produces a single or double rainbow on sunny days.

Seljalandsfoss is a waterfall that can be fully encircled, situated on the South Coast of Iceland with a drop of 60 metres (200 feet).

Due to the waterfall’s close proximity to the Ring Roadand impressive natural features, it is one the country's most famous and visited falls. Majestic and picturesque, it is one of the most photographed features in all of Iceland.

Geology and Surroundings

Seljalandsfoss waterfall, part of the river Seljalandsá, has its origins underneath the glacier Eyjafjallajökull. The volcano beneath this ice cap was the one that erupted in 2010 and caused havoc at airports across Europe.

Geysir is a famous hot spring in Haukadalur valley in South Iceland. Part of the ‘Golden Circle', Geysir gives its name to hot springs all over the world.

Though Geysir itself is hardly active anymore, the area features spectacular hot springs such as the powerful Strokkur, which spouts a vast amount of water every 10 minutes, around 15-20 meters into the air, Smidur and Litli-Strokkur.

North of Geysir are fumaroles, i.e. unlike the hot springs the emit hot water, only steam and gas emanate from these. You may be able to observe bright yellow stains at the fumaroles, this is native sulphur, which crysallizes from the steam. At the southern part of the geothermal area, called Thykkuhverir, you‘ll find various mud pots. Such mud pots are actually fumaroles that boil up through surface water/groundwater and may become steaming fumaroles during dry spells, rather than the usual boiling mudpots.

About 2 km from Geysir is an old preserved natural pool called Marteinslaug. One can bathe in it and it has room for 3-5 people at a time, but care should be taken, as the area around the pool is very delicate. The temperature is 39-43°C, depending on how you are positioned in the pool. The water is slightly muddy, as the pool is built on soil, and the bottom is slippery due to algae, so caution is advised.

In Haukadalur there has also been tree planting in recent times and today the forest Haukadalsskogur is one of the largest in South Iceland. Aspen, various types of pine, and other plants have been tried out there and experiments and research continue. We also recommend visiting the tree museum, built in the memory of forester Gunnar Freysteinsson. There are good paths and roads in the forest and the wood is specially designed to accommodate wheelchairs.

Haukadalur has been a church site since ancient time. The current wooden church was last rebuilt in 1938 but the variety and appearance of the church dates back to 1842, making it one of the oldest of its kind in Iceland.

Haukadalur is indeed a historical place. It was settled during the age of settlement and scholar Ari “The Wise“ Thorgilsson grew up there. The first pastoral school in Iceland was also built there.

For accommodation, Hotel Gullfoss is about 7 km from the Geysir area, and closer still is the Hotel Geysir.

Gullfoss ('Golden Waterfall') in Hvita river is one of the most beautiful and beloved waterfalls in Iceland and forms a part of the famous Golden Circle along with Thingvellir National Park and the Geysir geothemal area.

This mighty waterfall cascades 32 meters into the river gorge and you'll be able to stand close enough to feel the waterspray on your face. Hvita itself should not be missed by any fan of rafting, as it is one of the most popular rafting rivers in Iceland.

The glacier volcano of Eyjafjallajökull is notorious the world over for causing havoc to air travel in 2010, and stumping television anchors everywhere as they tried to pronounce it. 1651 metres (5427 feet) tall, it is one of the most dominant features of the South Coast.

Geography

The glacier of Eyjafjallajökull is approximately 100 square kilometres (39 square miles), making it the country’s sixth largest. It sits close to the fourth greatest, Mýrdalsjökull, which also conceals another notorious volcano, this one called Katla.

While Eyjafjallajökull’s eruption was huge and disruptive, it pales in comparison to the potential of Katla. Far more explosive, and under much thicker ice, an eruption here in unfavourable wind conditions could have worldwide consequences.

The magma chambers between both of these mighty volcanoes are connected, and, unfortunately for us, an eruption at Eyjafjallajökull is usually followed by one at Katla within a decade.

Eyjafjallajökull has many glacial outlets, the most famous being Gígjökull. Many rivers flow from its meltwater, and one of these falls into the beautiful South Coast waterfall, Seljalandsfoss, which it is possible to fully encircle.

Eruptions

Eyjafjallajökull’s most recent eruption was no doubt the most famous in Iceland’s history (although the honour really should go to Laki, the 1783-4 eruption of which caused an ash cloud so great that Europe fell into a famine that many historians believe led to the French Revolution). On March 27th, 2010, magma began to bubble from beneath the surface, and by April 14th, ash was starting to billow from the peak.

800 people were evacuated, in fears not of magma, but of equally dangerous glacial floods, which have decimated Icelandic towns in the past. Animals were ordered to be kept inside, and those with respiratory problems told they should also stay indoors.

Air travel across Europe was halted, as, by the evening of April 15th, the ash was already over the UK, Scandinavia, and parts of Germany. Holidaymakers were trapped, waiting for news, and would end up stuck for eight days; in Scotland and Ireland, there were even flights delayed in May due to lingering effects.

Thankfully, no one was injured, although the ash is thought to have caused respiratory issues for some in the south of the country. Many farms were also destroyed by the ash and floods, with some farmers still struggling to recover today.

Since settlement in 874, Eyjafjallajökull has also erupted in 900, 1612, and from 1821 to 1823. The latter released a huge amount of fluoride which is believed to have affected the bone health of humans and animals alike at the time.

Eyjafjallajokull today

Eyjafjallajökull is now entirely safe to visit and is seen on most tours of the South Coast in clear weather. In the town of Hvolsvöllur, there is a visitor’s centre on the volcano, which focuses on the experience of one family whose farm, Þorvaldseyri, was one of the many destroyed by the floods, lava and ash.

It is very unlikely that Eyjafjallajökull will erupt again any time soon, with hundreds of years between each eruption, but as mentioned, its neighbour Katla might start rumbling...

Dyrhólaey Peninsula is a 120-metre promenade famed for its staggering views of Iceland’s South Coast, as well as its historic lighthouse and wealth of birdlife. It is home to a rock arch of the same name.

Dyrhólaey, which translates to Door Hill Island, is of volcanic origin and was once an island before joining up to the Icelandic mainland. In ancient times, passing sailors used to refer to Dyrhólaey as ‘Cape Portland’.

It is also the southernmost part of the Icelandic mainland, making it a popular stop for sightseers travelling along the Ring Road, and can be found close by the coastal village of Vík í Mýrdal.

Dyrhólaey Arch

Dyrhólaey’s most instantly recognisable attraction is the promenade’s massive rock arch, a result of centuries of erosion. As a result, its name is in direct reference to this enormous arch. In fact, this natural feature is so large and dramatic that one daredevil pilot even flew through it, back in 1993. Boats can easily cruise through its opening.

Dyrhólaey Wildlife

Dyrhólaey has an abundance of birdlife, the most common year-round being Eider Ducks. Iceland’s favourite winged resident, the migratory Atlantic Puffin, can be found here from May to September.

It is one of the best places to reliably locate them, and one of the closest to Reykjavík after the islands in Faxaflói Bay which can be visited by boat from the Old Harbour.

While watching puffins, it is striking how little they seem to fear people, as they allow you to get very close. Be aware, however, they do not like to be touched, and if one flies off in a panic, the whole flock might follow it, so be respectful.

Features at and around Dyrhólaey

From your position atop the promenade of Dyrhólaey, you can enjoy staggering views over Iceland’s black sand beaches, complemented by the glittering waves of the Atlantic on one side, and distant mountainscapes to the other.

The most notable stretch of coast here is called Reynisfjara, renowned for its incredible geology, with the sea-stacks of Reynisdrangar jutting up out to sea. If you visit this beach while seeing Dyrhólaey as part of a South Coast adventure, be sure to follow the warning signs and stay away from the water as dangerous sneaker waves here are commonplace.

To the north, you will also able to see the creeping glacier, Mýrdalsjökull. This amazing ice cap conceals a secret; beneath its surface is one of the most explosive and notorious volcanoes in all of Iceland, Katla. Long overdue, experts say that it is a matter of when - not if - it will erupt over the coming years.

On top of Dyrhólaey stands Dyrhólaeyjarviti, a beautiful old lighthouse that consists of a white, square concrete tower. The first lighthouse in the area was built in 1919; the current construction was completed in 1927. Visitors here will be able to see the lighthouse flicking out beams of white light to sea every ten seconds.

Geography

The first thing that visitors to the National Park notice is its sheer aesthetic beauty; dried magma fields, covered in Icelandic moss, sit carved by glacial springs and surrounded by a bowl of ancient mountain peaks.

Two of the greatest attractions in the park are the exposed North American and Eurasian tectonic plates; it is one of the only regions in the world where you can see geology such as this on land.

Visitors are encouraged to walk along the North American tectonic plate, where they can read more about the area’s fascinating formation and history, before descending into the valley below.

History

Þingvellir can be anglicised to ‘Fields of Parliament’, a nod to the area’s fascinating history and relevance to Icelandic culture. It is here, after all, that the world’s first democratically elected parliament that remains functioning, Alþingi, was formed in 930 AD.

It may seem unlikely that Vikings would want to be under such an uncombative government, but the thirty or so clans that lived in Iceland at the time sought to prosper in their harsh new environment.

The first gathering was such a success that the meetings became annual, and it became a place where disputes were settled, criminals were tried, and laws to the benefit of all were laid down.

This saw the birth of the Icelandic Commonwealth, a time of independence and freedom for the Icelandic people before they became constituents of the Norwegian monarchy. Sessions would continue to be held at Þingvellir until 1798.

Though the parliament was removed by the Danish at this time, it returned 1845 to Reykjavík.

Another major reason as to why Þingvellir is considered so important to Icelanders is the fact that this is where the decision was made to abandon the belief of Paganism and the Norse Gods; the people adopted Christianity in 1000 AD under threat of invasion from Norway.

This turning point in history was left to the pagan lawspeaker, Þorgeir Þorkelsson, who rested on the choice for one day and one night before reappearing to share his decision.

To symbolise the country’s change, he threw idols of his old deities into the northern waterfall Goðafoss, the name of which translates to ‘Waterfall of the Gods’.

Silfra Fissure

Þingvellir is one of the most widely visited attractions in Iceland, in large part due to the fact that it is home to the glacial spring, Silfra fissure, one of the top ten sites in the world for snorkellers and scuba divers.

Silfra (meaning ‘Silver’) is a submerged ravine within the park, boasting visibility of up to 100 metres (328 feet) and a temperature just above freezing. Participants in these tours will be attired at the Silfra carpark in neoprene hoodies and gloves, as well as an undersuit and drysuit for thermal protection.

Strokkur is found in the Geysir Geothermal Area, titled after the Great Geysir, which lent its name to all others across the world. It is the greatest active geyser on site; Geysir itself is in a period of inactivity. Strokkur erupts more regularly than Geysir ever did, blasting water to heights of around fifteen to twenty metres every five to ten minutes, although it is known to reach up to forty metres.

Strokkur and Haukadalur Valley

Strokkur is the primary feature of the Haukadalur valleyand the main reason why it is one of the most visited sites in the country. While Geysir will very occasionally still erupt to enormous heights, it is nowhere near reliable enough to justify the area’s popularity.

Haukadalur valley, however, has many other features that make it worth a visit. The natural beauty of the area is shaped by the forces of the earth; fumaroles, hot-springs, mud-pits and other little geysers are littered around, and the ground itself is dyed vividly by elements such as sulfur (yellow), copper (green) and iron (red).

Opposite the main geothermal area in Haukadalur Valley is a restaurant, cafe, hotel and luxury gift shop.

Science behind Strokkur

Active geysers like Strokkur are rare around the world, due to the fact that many conditions must be met for them to form. They are thus only found in certain parts of highly geothermal areas.

The first condition that is necessary is an intense heat source; magma must be close enough to the surface of the earth for the rocks to be hot enough to boil water. Considering that Iceland is located on top of the rift valley between the North American and Eurasian tectonic plates, this condition is met throughout most of the county.

Secondly, you will need a source of flowing underground water. In the case of Strokkur, this comes from the second largest glacier in the country, Langjökull. Meltwater from the glacier sinks into the surrounding porous lava rock, and travels underground in all directions.

Evidence of this flowing water can be found in Þingvellir National Park, where there are many freshwater springs flowing straight from the earth.

Finally, you need a complex plumbing system that allows a geyser to erupt, rather than just steam from the ground like a fumarole. Above the intense heat source, there must be space for the flowing water to gather like a reservoir. From this basin, there must be a vent to the surface. This vent must be lined with silica so that the boiling, rising water cannot escape before the eruption.

Environmental Issues with Strokkur

One of the main reasons that Geysir entered a period of inactivity was due to the fact soap used to be pumped into the vents to make the eruptions more dramatic; it damaged the structure of the vent and prevented water building up. Strokkur, therefore, is guarded against all interference, with chains keeping visitors a good distance away.

Unfortunately, however, there have been incidents where people have meddled with its natural state. For example, an artist called Marco Evaristti once poured food colouring into it to make the eruption pink. He defended himself by claiming that nature was open to artists to utiltise and the fact the colouring was all-natural, but he became a pariah amongst many Icelanders, and was arrested and fined (though never paid it).

Volcanic & Geothermal Activity

The Reykjanes Peninsula runs along the Mid-Atlantic Rift, where the Eurasian and the North American tectonic plates are drifting apart. Due to this geological setting, the whole peninsula is extremely volcanically active, covered with lava fields, and eruptions and earthquakes are very common here.

During the Middle Ages, many eruptions occurred in Reykjanes, but no eruptions have been recorded here for the last 500 years. This is simply a period of dormancy, however; they could start again at any time.

Earthquakes are still common. In 2001, one occurred beneath the lake Kleifarvatn and drained it to the extent that it lost 25 per cent of its surface area. Since then, hot springs have been bubbling beneath its surface.

The main geothermal areas of Reykjanes, however, are Gunnuhver, Krýsuvik and Svartsengi. Various mud pools and fumaroles can be seen at Gunnuhver, while Krýsuvik is characterised by hot springs and mud pots that bestow multicoloured hues upon the soil.

Nature & Wildlife

Reykjanes' cliffs are teeming with birdlife. Its best-known bird colony resides in Krýsuvikurbjarg which is the nesting place of approximately eighty thousand seabirds. While puffins are not found here, it is an excellent place to spot cormorants, fulmar, and other such species.

North of Krýsuvíkurbjarg is the aforementioned Kleifarvatn, the largest lake on the peninsula and one of the deepest in Iceland. On the centre of the peninsula is lake Djúpavatn, a popular fishing destination.

Reykjanes is hammered by some of the most breath-taking breaker waves in the world. A short drive from Krýsuvík is Selvogur, where one can witness mighty waves shattering against the rocks. On Reykjanestá, the southwest tip of the peninsula, the waves are known to reach heights of thirty metres (nearly one hundred feet).

Because of this, coastal erosion is constantly ongoing at Reykjanes, and if it were not for the eruptions, it would either be much narrower or simply lost to the seas.

The peninsula's north side is dotted with fishing villages and towns, most notably Keflavík, Sandgerði, Garður and Vogar. Grindavík town is located on the south shore of the peninsula. Together, the towns and towns Keflavík, Njarðvík, Hafnir and Ásbrú make up the municipality Reykjanesbær which consists of just under 16,000 residents, making it the fifth largest municipality in Iceland.

Miðnesheiði

Near Keflavík is the Miðnesheiði heath, where the international airport, Leifsstöð (also known as Keflavíkurflugvöllur, or Keflavík Airport) is located. This is the port of arrival for the vast majority of travellers coming to Iceland.

The World-Famous Spa

On the southern tip of the peninsula is the Blue Lagoon geothermal spa, an ideal place for relaxing and bathing and one of the most-visited attractions in Iceland.

Hvalfjörður is a fjord in southwest Iceland. The fjord is approximately 30 kilometres (19 miles) long and five (three miles) kilometres wide.

Nature and Landscape

The landscape of Hvalfjörður is varied and beautiful, with wide areas of flat land along majestic mountains, green vegetation in summer and beaches cut with creeks.

The area is rich in bird life and is home to seals, but despite its name, which translates to ‘Whale Fjord,’ it is not known for its whale or dolphin populations. Two theories exist on how it got its name; either that it was once home to whales before fish stocks moved away, or because of the general shape of the bay.

The area has recently been part of Iceland’s successful reforestation effort.

Natural attractions in the area are plentiful but most significant is Iceland's highest waterfall, Glymur, in the river Botnsá. There are also plenty of interesting hiking trails in the area, such as Síldarmannagotur, leading north, and Leggjabrjótur, leading east towards the area of Þingvellir National Park.

History and Culture

Historically, Hvalfjörður was home to one of the main whaling stations in Iceland, with ships heading out into Faxaflói Bay. It was one of the most important naval stations in the North Atlantic during World War Two, when Iceland was occupied by the Allies after the Nazis conquered Denmark.

The old whaling station and a war museum can be found in the fjord.

Iceland's main psalm poet, Hallgrímur Pétursson, writer of the ‘Passia Hymns,' lived in Hvalfjörður. The area was also the home of the late Sveinbjörn Beinteinsson, poet and performer and head of the Icelandic Pagan Association.

Economy

Most inhabitants of the fjord live in rural areas, and there is some farming in the area. Until the 1990s those travelling between Borgarnes and Reykjavík had to take a long detour around the fjord, but this was solved with a tunnel that travels beneath it, finished in 1998.

Grundartangi promontory in Hvalfjörður has one of the largest harbours in the country and two industrial plants. One is a ferrosilicon plant, operated since 1979, the other an aluminium smelter, operated since 1998.

Both of these were controversial during their construction, and continue to be controversial during their ongoing operation. Along with whaling and hydroelectric dams, smelters and silicone plants are the hottest environmental debates going on in Iceland.

Mýrdalsjökull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest ice cap, covering nearly 600 square kilometres (232 square miles), and its highest peak is almost 1500 meters tall. It is most well-known for sitting atop the notorious and explosive volcano, Katla.

Mýrdalsjökull is visible from Route 1 on the South Coast, sitting to the north of the village of Vík. It is visited on some snowmobiling, ice caving and helicopter tours, and one of its glacial outlets, Sólheimajökull, is the most popular place in the country for ice-climbing and glacier hiking.

Eruptions beneath Myrdalsjokull

Since 2010, the world has known of the volcano beneath Eyjafjallajökull; after all, it halted European air travel for over a week and stumped news readers everywhere. Few, however, are aware of the much larger volcano right beside it.

Mýrdalsjökull conceals Katla, one of the country’s most active volcanoes, having erupted, on average, once every fifty years since 930 AD. Because of the glacier above it, these eruptions tend to cause enormous ash clouds. It is these ash clouds that lead to flights being grounded, crops and livestock poisoned, and have the potential to change the world’s climate.

The last major eruption beneath Katla was in 1918, in which such huge lahar floods occurred that the southern coastline was extended five kilometres outwards. This area is also very susceptible to glacial floods, or 'jökulhlaup', during eruptions, even when the lava does not break through the surface of the ice. These are as dangerous as the lava itself, having wiped out whole Icelandic villages before.

Historically, the area was little settled for this reason.

Katla is connected to the same volcanic system as Eyjafjallajökull and usually erupts violently a few years after Eyjafjallajökull does. As the ex-president, Ólafur Ragnar Grímsson said in 2010:

‘The time for Katla to erupt is coming close… it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption’

So it is currently several years overdue. Katla is monitored heavily, and roads around it closed when seismic activity increases. All road closures around Iceland can be found on Road and Coastal Administration's website.

Tours on Myrdalsjokull

While there are no eruptions immediately imminent, tours continue to run onMýrdalsjökull, allowing visitors to enjoy the glacier. It is, for example, possible to snowmobile across its surface throughout the year and take ice caving tours beneath it from October to April, with departures from both Reykjavík and Vík.

Considering the ice caves under Vatnajökull glacier are usually only accessible from November to March, this provides a wider window of opportunity for travellers to Iceland outside of the depths of winter. It should be noted that the caves in Mýrdalsjökull do not have the same blue ice, however.

Tours around Myrdalsjokull

Mýrdalsjökull can be seen on all South Coast tours that reach Vík and beyond in clear weather. It can also be seen from above on helicopter tours that depart from Reykjavík.

The best perspectives of the glacier, however, can be found on the popular Fimmvörðuháls hiking trail, which goes between Eyjafjallajökull and Mýrdalsjökull. Part of this hike can be done in a day, or you can take the complete route from Þórsmörk to Skógar on a three-day trek

Sólheimasandur is a vast area of sand and gravel along the South Coast of Iceland, between the cliffs of the interior and the modern shoreline. It was built up by immense glacier bursts sweeping from the mountains to the shore.

Geography of Sólheimasandur

Sólheimasandur is a glacial outwash plain, meaning when that when eruptions happen under the nearby glacier, Mýrdalsjökull, the floodwater rushes across this land for the sea.

A glacial flood, otherwise called Jökulhlaup (one of two words taken from Icelandic in the English language, the other being geyser) is perhaps the most dangerous immediate element of an Icelandic eruption. While individuals have been killed by lava flows and bombs, many more have lost their lives to the water.

For this reason, Sólheimasandur has no significant settlements, all the way from the village of Vík í Mýrdal to Kirkjubæjarklaustur. The whole area is vulnerable to glacial floods, which are still notoriously unpredictable to modern science.

This is especially the case considering that the volcano beneath Mýrdalsjökull, Katla, is Iceland’s most active volcano, which carries a reputation for violently erupting, seemingly at random.

Even if these eruptions do not break the surface of the ice, they can still cause devastating floods. In fact, these can even be more dangerous, as these eruptions are often not detected..

If Katla is showing signs of waking, then the Ring Road going south across Sólheimasandur is often closed.

In spite of its dark reputation, Sólheimasandur is a place of ethereal and haunting beauty. Entirely flat, composed of black sands, it is often compared to a lunar landscape, or else some kind fantastical desert. The views of Mýrdalsjökull, Vatnajökull, the Highlands and the South Coast are also magnificent in clear weather.

Sólheimasandur is easy to reach, laying on the Ring Road that encircles the country.

The DC-3 Plane Wreckage

One of the most impressive sights on Sólheimasandur is the DC-3 plane wreckage. Lying abandoned in the sand, a deteriorating skeleton, with nothing but endless black sand surrounding it, it makes an eerie destination even more ominous.

It is a US Navy plane, that was flying across the area in 1973; until recently the US had a NATO base at Keflavík, as Iceland has no armed forces of its own. It seemed to run out of fuel - although it was later discovered that the pilot had, in fact, switched to the wrong fuel tank - and had to make an emergency landing.

Thankfully, no one was killed or injured, although the plane was far too damaged to be repaired.

Because there were no deaths or injuries, there is nothing tasteless about taking photos with the plane. In fact, it a popular addition to many South Coast tours. Because the wreckage is not expected to remain there for long - considering the regular glacial floods that rush through the area - it is fine to touch it. It is not recommended that you climb on it, however, for safety reasons.

Hveragerði is a town and municipality in the southwest of Iceland. It is often nicknamed ‘the Earthquake Town’ or ‘the Hot Spring Town’, due to the active geological and geothermal forces that define it.

Hveragerdi town and services

Hveragerði is around 45 kilometres (28 miles) from the capital Reykjavík and takes half an hour to drive to along the Ring Road travelling south. Around 2,300 people live in Hveragerði, most employed in tourism, horticulture or agriculture.

There is a service centre in the town with shops, including an alcohol shop, a supermarket, a gas station, an information point, and a cafe. There are several restaurants as well, and just outside it is a popular horse farm.

Surrounding the town are nice botanical areas and many recreational activities are available. There are excellent hiking trails as well as nice hotels and a camping ground which is open in the summer months.

In terms of culture, a number of museums can be found in Hveragerði, such as the Árnesingar art museum and Hveragerði Stone and Mineral Museum. The town even hosts an annual culture and family festival in August.

Geography of Hveragerdi

Hveragerði sits on a highly geothermal area. Boiling water runs just beneath the surface of the ground, leading to many hot springs in the nearby hills. This is both a blessing for the town and a curse.

In terms of a blessing, it allows greenhouses to flourish, as they can be provided with heat throughout the year. Hveragerði is thus the world’s northernmost producer of bananas, which are grown alongside a host of other fruits and vegetables.

Many flowers and herbs are also grown here, and it is considered the centre of botany in Iceland.

The boiling water also allows food to be cooked simply by burying it for a few hours, providing the restaurants in the area with unique menus. It also brings the area a wealth of tourism.

The curse of this geothermal water is the effect it has on the residents. Stories of hot springs opening overnight in people’s kitchens, bedrooms and living rooms are very common.

Also, due to the Mid-Atlantic rift running through Iceland, many earthquakes hit Hveragerði. Fortunately, the houses are built here to withstand tremors, due to how common they are, but there is a lingering knowledge that a powerful earthquake or eruption could cause serious, perhaps irreparable damage to the settlement.

The river Varmá runs from the valley of Reykjadalur through the town. This region, which translates to the 'Steam Valley', is an incredibly popular place for hot spring bathing and hiking.

A gravel road that leads from Hveragerði takes you to the base of the hiking trail, which winds up, down and around beautiful, scenic hills dotted with fumaroles and mud pits.

It ends by a river that is fed by hot springs, meaning it is heated from the top, allowing visitors to choose the perfect place to bathe. There are no indoor changing areas, but screens to undress behind.

Reynisfjara is a black pebble beach and features an amazing cliff of regular basalt columns resembling a rocky step pyramid, which is called Hálsanef. Out in the sea are the spectacularly shaped basalt sea stacks Reynisdrangar. The area has a rich birdlife, including puffins, fulmars and guillemots.

The waves at Reynisfjara are especially strong and unpredictable, and fatal accidents have occurred at this beach, so people are advised to take extra care when visiting the area.

According to folklore, two trolls attempted to drag a ship to land but were turned to stone as daylight broke, turning them into the Reynisdrangar stacks, clearly visible from the beach.

Vík í Mýdral, or just Vík, is the southernmost village on the Icelandic mainland, located 186 kilometres (110 miles) from the capital Reykjavík.

Often visited by those travelling the popular sightseeing route along the South Coast, it is a wonderful place to stop, recharge, and if you are taking your time, rest for the night. Though it only has around 300 residents, the village is very popular amongst tourists for its convenience and beautiful surrounding landscapes.

Features near Vik

Reaching Vík from Reykjavík takes approximately two and a half hours, and en route, there are many marvellous features to admire. Two of the country’s most famous waterfalls, Skógafoss and Seljalandsfoss, lay between the two destinations; the former has awe-inspiring power, whereas the latter can be fully encircled.

The glaciers Eyjafjallajökull and Mýrdalsjökull can also be seen on clear days; both of these cover volcanoes which are particularly explosive, with Eyjafjallajökull famously disrupting European air travel in 2010. Out to sea in especially good weather, the Westman Islands can also be seen on the horizon.

Just before Vík are the popular birdwatching cliffs of Dyrhólaey, where you can also find an enormous rock arch curving out into the ocean. This is one of the best places for birdwatching in Iceland, with thousands of puffins nesting here from May to August.

The village itself sits opposite one of the country’s most famous features: Reynisfjara black sand beach. Considered one of the world’s most beautiful non-tropical beaches, it boasts incredible geology.

Particularly of note are the Reynisdrangar sea-stacks, said to be two trolls frozen in the light of the morning sun as they tried to pull a ship into shore.

Though this beach makes for a lovely walk, particularly for those staying in Vík overnight, as they can see it under the midnight sun or northern lights, it has its dangers. Sneaker waves can be notorious here, so visitors should stay far from the water’s edge, and never go for a swim. Lives have been lost here before.

The route to Vík from Reykjavík is beautiful and continues to be so as you travel further along the South Coast, through the Skeiðarásandur black-sand-plains into Vatnajökull National Park. This beautiful region is often the final destination of those passing through Vík, as it is home to the largest glacier in Europe, the Skaftafell Nature Reserve, and Jökulsárlón Glacier Lagoon.

Of course, ambitious travellers will carry on from here to encircle the full country.

Wildlife around Vik

Vík, due to its closeness to the Reynisfjall and Dyrhólaey cliffs, has a rich birdlife. Short walks from the village will take you to the nesting grounds of gulls, fulmar, guillemots, and in summer, puffins.

Due to its coastal location, visitors to Vík have a decent chance to see seals on the shore. There is also a slim chance to see whales or dolphins; the twenty or so species that live in Iceland’s waters can appear at any time.

Services in Vik

Vík has a wide variety of public services, due to its remoteness and its importance in connecting the east and west of Iceland. There are gas stations, shops and cafes, a swimming pool, a wool factory that can be visited, and a wide range of accommodation options for all budgets.

Please note, however, that as the village has such a small year-round population, those with special dietary requirements should purchase their food from Reykjavík before departing.

Kerid is a volcanic crater lake in Grimsnes in South Iceland. It is a popular stop when traveling the Golden Circle.

It is believed that Kerid was originally a cone volcano that erupted and and emptied its magma reserve. Once the magma was depleted, the weight of the cone collapsed into an empty magma chamber, later to be filled with water.

The Kerid caldera is composed of red volcanic rock and is around 55 m deep, 170 m wide and 270 m across. There is little vegetation in the steep-walled crater, save for one wall with a gentler slope which is covered with deep moss. This wall is fairly easy to descend.

The lake itself is fairly shallow and is striking in its beauty. Opaque and aquamarine, surrounded by the red crater walls, Kerid offers a great contrast of colours and a highly impressive scenery.

Öxarárfoss is a waterfall situated within Þingvellir National Park in southwest Iceland.

The waterfall flows out the river Öxará, cascading in two drops over the cliffs of Almannagjá gorge, which marks the eastern boundary of the North American and Eurasian tectonic plates.

Description

The waterfall has a height of 13 metres (44 feet) and an average width of six metres (20 feet). The pool of water at the waterfall’s base is dotted with large, smooth rocks, which get especially icy in winter. The waterfall can be visited year round, but expect large crowds during the peak season of the summer.

During the depths of winter, the waterfall is entirely frozen over. Ice climbers have been known to scale it, but this should only be done with and by experts.

The geological reason is that, as mentioned, Þingvellir lies between the tectonic plates. As they pull apart, the land is torn, and thus there are many beautiful ravines and lava fields to be found.

The most famous of these ravines is Silfra. Like the others, it is filled with crystal clear glacial water, which emerges from a spring, but unlike the others, it is possible to take snorkelling and diving tours here.

The water from the crevasses such as Silfra feed into the lake Þingvellavatn; in fact, the river Öxará, which feeds Öxarárfoss, is the only source of the lake that does not come from a spring.

The historical reason that makes Þingvellir so famous is that it was the original site of the Alþing, the Icelandic parliament founded in 930 AD. This parliament continues to exist in Reykjavík but for nine centuries flourished here.

Icelanders would meet annually to pass laws, settle disputes, and share news. It was both incredibly progressive, giving a voice to all people and granting women divorces long before many other nations were considering it, and barbaric, hosting many battles and the prosecution of dozens of witches.

It is thus featured in many sagas, and though not always mentioned in them, Öxarárfoss was a witness to this long history.

One notable piece of folklore about the waterfall was that it was said to have prophetic powers for the year ahead. At midnight on New Years Eve, it would run red with either wine or blood, with the former promising prosperity ahead, and the latter warning of war.

The South Coast of Iceland is the country's most visited sightseeing route, along with the Golden Circle.

This incredible shoreline stretches from the greater Reykjavík area in the west to the magnificent Jökulsárlón glacier lagoon in the east and is lined with countless natural wonders such as cascading waterfalls, volcanoes, black sand beaches and glaciers.

Geography, Nature & Wildlife

The South Coast is the most easily accessible part of the country’s southern region, found along the Route 1 highway (the Ring Road), which encircles Iceland. The area consists of a diverse lowland that transitions between, marshlands, bays, cultivated pastures, estuaries and black sand deserts.

Underneath the soil rests a vast lava field, known as Þjórsárhraun. Its edges reach several hundred metres offshore where the ocean waves crash upon them, thereby protecting the lowland from the invasion of the sea. This results in the South Coast being unusually lacking in the deep fjords that so distinctly characterise the rest of Iceland's shoreline.

The region boasts vibrant bird life during all seasons. Freshwater birds nest in the marshlands and around the estuaries, while seabirds flock around the cliffs of Reynisdrangar and Dyrhólaey, including the North Atlantic puffin between May and August. Some species stay throughout the harsh Icelandic winter, including the northern diver, the loom and various species of gulls and ducks.

Seals are often found along the shore, particularly around the Jökulsárlón Glacier Lagoon and Diamond Beach. As with everywhere in Iceland, you should always keep an eye out to sea, as whales and dolphins reside all along its coastline.

Highlights of the South Coast

When driving the route from Reykjavík city, the first major features are the two great waterfalls of Seljalandsfoss and Skógafoss, which sit beneath the notorious subglacial volcano, Eyjafjallajökull. On clear days from these beautiful cascades, the Westman Islands can be seen across the ocean.

A little further down the route is the glacier Mýrdalsjökull, which covers one of Iceland’s most explosive volcanoes, Katla. Many glacier hikes are taken here upon the outlet of Sólheimajökull.

The aforementioned Dyrhólaey cliffs are next, home to many seabirds. Even if you come outside of puffin season, they are well worth a visit; jutting out to sea is an enormous rock arch of the same name, which you can marvel at from many angles.

Adjacent to the village of Vík is the famous black-sand beach, Reynisfjara, home to the rock pillars of Reynisdrangar, said to be two trolls frozen by the light of the sun. Though beautiful, this area is gaining notoriety for its dangerous sneaker waves, so visitors should be sure to stay well away from the edge of the water, even on a calm, still day.

There are no landmasses between Reynisfjara beach and the continent of Antarctica, so you can imagine how the waves can build momentum.

After passing through Vík, you will cross the glacial sand plain of Skeiðarársandur, before entering Vatnajökull National Park, home to the largest ice cap in Europe, Vatnajökull itself, dozens of glacial outlets and the magnificent Jökulsárlón glacier lagoon.

While almost all of these sites can be seen from Route 1, they make up a fraction of what the South Coast has to offer. The vast sand plains of Sólheimasandur are home to a crashed DC-3 Plane Wreck, and within the Vatnajökull National Park is the dramatic Skaftafell Nature Reserve.

Less than a kilometre from Seljalandsfoss is the hidden gem of Gljúfrabúi waterfall, and short distances from Jökulsárlón you will find the Diamond Beach, where icebergs wash on the black-sand shore, and another glacier lagoon, Fjallsárlón.